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The Kengdenongshe giant Au-Ag-Pb-Zn polymetallic deposit in the East Kunlun Orogen contains significant quantities of metals, including 42.2 t of Au and 1.05 Mt of Pb and Zn, primarily hosted in Late Permian to Triassic rhyolitic tuff. The deposit features two types of ore bodies: Pb-Zn rich and Au-Ag rich, with distinct mineral compositions and hydrothermal alteration patterns, indicating a volcanic-associated massive sulfide (VMS) origin. Geological, fluid inclusion, and isotope analyses suggest a mixed m

Author
jshcugb
Language
EN